{"refrec":{"BRefID":210750,"RR":"<b>Prowe, A.E.F.; Thomas, H.; Patsch, J.; Kuhn, W.; Bozec, Y.; Schiettecatte, L.S.; Borges, A.V.; de Baar, H.J.W.</b> (2009). Mechanisms controlling the air-sea <i>CO<sub>2</sub></i> flux in the North Sea. <i>Cont. Shelf Res. 29(15)</i>: 1801-1808. <a href=\"http://dx.doi.org/10.1016/j.csr.2009.06.003\" target=\"_blank\">dx.doi.org/10.1016/j.csr.2009.06.003</a>","BEntID":202672,"PublicFlag":1,"CheckedFlag":1,"wosflag":1,"vabbflag":1,"RefStringPartII":". <i>Cont. Shelf Res. 29(15)</i>: 1801-1808. <a href=\"https://dx.doi.org/10.1016/j.csr.2009.06.003\" target=\"_blank\">https://dx.doi.org/10.1016/j.csr.2009.06.003</a>","DocTypID":8,"DocType":"Journal article","MarineFlag":1,"FreshFlag":0,"BrackishFlag":0,"TerrestrialFlag":0,"Authorstring":"Prowe, A.E.F.; Thomas, H.; Patsch, J.; Kuhn, W.; Bozec, Y.; Schiettecatte, L.S.; Borges, A.V.; de Baar, H.J.W.","OrigTitleTranslFlag":0,"Authorstringtrunc":"Prowe, A.E.F. <i>et al.</i>","Englishabstract":"The mechanisms driving the air-sea exchange of carbon dioxide (CO<sub>2</sub>) in the North Sea are investigated using the three-dimensional coupled physical-biogeochemical model ECOHAM (ECOlogical-model, HAMburg). We validate our simulations using field data for the years 2001-2002 and identify the controls of the air-sea CO<sub>2</sub> flux for two locations representative for the North Sea's biogeochemical provinces. In the seasonally stratified northern region, net CO<sub>2</sub> uptake is high (2: 06 mol m<sup>-2</sup> a<sup>-1</sup>) due to high net community production (NCP) in the surface water. Overflow production releasing semi-labile dissolved organic carbon needs to be considered for a realistic simulation of the low dissolved inorganic carbon (DIC) concentrations observed during summer. This biologically driven carbon drawdown outcompetes the temperature-driven rise in CO<sub>2</sub> partial pressure (pCO<sub>2</sub>) during the productive season. In contrast, the permanently mixed southern region is a weak net CO<sub>2</sub> source (0:78 mol m<sup>-2</sup> a<sup>-1</sup>). NCP is generally low except for the spring bloom because remineralization parallels primary production. Here, the pCO<sub>2</sub> appears to be controlled by temperature.","AbstractOtherLang":null,"BibLvlCode":"AS","StandardTitle":"Mechanisms controlling the air-sea <i>CO<sub>2</sub></i> flux in the North Sea","OrigTitleLangCode":"en","OrigTitleLangCodeExtended":"eng","OrigTitleLangID":15,"DateLastModified":{"date":"2024-12-10 01:33:17.368041","timezone_type":1,"timezone":"+01:00"},"UserAccessRight":null,"UserAccID":null,"AuthorKeywords":"CO<sub>2<; sub> air-sea flux; Continental shelf pump; Biogeochemical modelling;","OtherDescriptors":null,"Notes":null,"AnaPub":2009,"MonPub":null,"DateUpdate":"2012-01-10","DateCreate":"2011-12-22","SecASFANote":null,"ConfID":null,"PeerRev":1,"VlizCoreFlag":1,"WoScode":"WOS:000273061800004","VABBcode":null,"OpenAcc":0,"DOI":"10.1016/j.csr.2009.06.003"},"refs":null,"anarec":{"AnaID":210750,"PubliDate":2009,"Pagination":"1801-1808","XtraPublOfAnaID":null,"ISBN":null,"Volume":"29","Issue":"15","BRefMon":null,"BRefMonRR":null,"BRefXtra":null,"BRefXtraRR":null,"SerBRefID":42769,"SerRR":"Continental Shelf Research. 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